首页|2021年秋汛期三门峡水库潼三区间来水量研究

2021年秋汛期三门峡水库潼三区间来水量研究

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2021 年黄河发生 1949 年以来最严重秋汛,三门峡水库在此次秋汛防洪调度中发挥了重要的作用.由于潼关至三门峡区间(潼三区间)缺乏水文监测,因此在 2021 年秋汛期以潼关站计算的入库水量与实际水量相差 10.4 亿m3,对区间来水考虑不足影响了三门峡水库的精准调度.从库区区间来水分析着手,以潼三区间为研究对象,根据数字高程模型、土地利用类型、土壤类型、气象水文等数据,建立了HEC-HMS分布式水文模型,选取包括 2021 年秋汛在内的 11 场实测洪水资料进行率定和验证.结果表明,11场洪水模拟洪峰流量误差均小于 20.0%,平均确定性系数为 0.725,模拟合格率为 90.9%,较准确地模拟了 2021 年秋汛期潼三区间来水过程,并量化了不同支流对区间来水总量的贡献率.
Analysis of the Inflow of Water from Tongguan-Sanmenxia Reach of Sanmenxia Reservoir During Autumn Flood Season in 2021
In 2021,the Yellow River experienced the most serious autumn flood since 1949.The Sanmenxia Reservoir played an important role in the autumn flood control,but there was 1.04 billion cubic meters difference between the inflow and outflow of the flood volume.In order to identify the cause of the above water imbalance,this paper took Tongguan-Sanmenxia reach as the study area,and digital elevation model,land use,soil type,meteorological and hydrological data were used to drive a HEC-HMS distributed hydrological model for flood processes simulation.The results show that the bias of simulated flood peak in 11 floods are all less than 20.0%,the average coefficient of determination of the simulations is 0.725,and the pass rate of the results is 90.9%.The model accurately simulates the water inflow process in the Tongguan-Sanmenxia reach during the au-tumn flood season in 2021,and the contribution of different tributaries to the total flood amount of the reach is quantified.

HEC-HMS modelflood compositionSanmenxia Reservoirwatershed of Tongguan-Sanmenxia reach

杨志豪、谷苗苗、钟家淦、王雪莹、王晓燕

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河南省三门峡水文水资源勘测局,河南 三门峡 472000

河南省洛阳水文水资源勘测局,河南 洛阳 471011

河海大学 水文水资源学院,江苏 南京 210098

HEC-HMS模型 洪水组成 三门峡水库 潼三区间流域

国家自然科学基金资助项目

42277074

2024

人民黄河
水利部黄河水利委员会

人民黄河

CSTPCD北大核心
影响因子:0.494
ISSN:1000-1379
年,卷(期):2024.46(7)